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naturally produced (Marsh and Minckley 1989b, Minckley et al. in <br />press). <br />Gila River--Most warmwater reaches of the Gila River <br />drainage in Arizona historically supported razorback suckers. <br />Records for the species in the Gila River downstream of the Gila- <br />Salt River confluence were uncommon probably because of <br />dewatering and a lack of collections prior to 1960 (Minckley <br />1973). In the Gila River upstream of the Salt River, and in the <br />San Pedro River (a tributary of the Gila River), historic <br />collections of razorback suckers were also uncommon, perhaps due <br />to low collecting effort prior to 1940 (Minckley 1973). The few <br />reports available, however, suggested that it was common in the <br />Gila River nearly to the New Mexico border (Kirsch 1889) and was <br />available in marketable quantities upstream in the San Pedro <br />River (Miller 1955, 1961). <br />Razorback suckers were abundant in the lower Salt River <br />downstream of present-day Roosevelt Lake, and also occurred in <br />the Verde River to near Perkinsville, Arizona (Minckley 1973), <br />and in lower Tonto Creek (Hobbs and Miller 1953). Historically, <br />razorback suckers "ran" up irrigation ditches and canals in <br />Arizona, and were so common that they, and the federally <br />endangered Colorado squawfish, Ptychocheilus lucius, were <br />pitchforked onto agricultural fields for fertilizer (Minckley <br />1973). The upstream distribution of razorback suckers in the <br />Salt River may have been limited by extensive canyon habitat. <br />Razorback suckers also used smaller streams, especially in <br />13 <br />